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\begin{document}

\title{Relationship between the tropical tropopause and tropical easterly jet
streams over Indian monsoon region}



\author[1]{Sanjay K. Mehta}%
\author[2]{Vanmathi A}%
\author[2]{Saleem Ali}%
\author[2]{Aravindhavel A}%
\author[3]{Ramesh Reddy}%
\affil[1]{SRM Research Institute}%
\affil[2]{SRM Research Institute, SRM IST}%
\affil[3]{SRM Reserach Institute, SRM IST}%


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  \date{May 27, 2024}


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\begin{abstract}
This paper presents the first quantitative relationship between the cold
point tropopause (CPT) and tropical easterly jet (TEJ) using radiosonde
observations over Gadanki (13.45oN, 79.2oE) during the Indian summer
monsoon season 2006--2014. CPT and TEJ peak altitudes (H\_CPT and
H\_TEJ) show amalgams of two categories of variability on day to day
scale. In category1 H\_TEJ occurs close to H\_CPT and they show in phase
variation. While in category2 H\_TEJ occurs far apart from H\_CPT and
they do not show any relationship. For category1 H\_CPT and H\_TEJ are
strongly correlated (0.70) as well as H\_CPT and T\_CPT (CPT
temperature) are moderately anticorrelated (-0.55) significant at 95\%
confidence level indicating the dominance of adiabatic processes.
Whereas in category2 H\_CPT and T\_CPT are not significantly
anticorrelated. Thus, when TEJ and CPT are close to each other it may
serve as an indicator for the prevalence of synoptic-scale effect.%
\end{abstract}%



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